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- W70950068 abstract "In general, it is accepted that primary loess deposits are undifferentiated and consequently are not laminated or bedded. Redeposition by running water, after primary eolian sedimentation, can produce laminated deposits. Redeposition by splash action only, produces undifferentiated deposits. This experimental study is focussed on the relationship between the moisture conditions at the depositionary surface (i. e. dry, moist, wet or under water) and the resulting sedimentary structures formed in silt loam deposits at various wind velocities and during calm periods. Sedimentation during calm periods, so-called fall-out, is simulated in a 7 metres high vertical column. Deposition at various wind velocities is simulated in a wind tunnel. Micromorphic investigations of thin sections suggest that during fall-out only weakly developed intercalated laminae are produced in loess deposited under water. In the wind tunnel laminated deposits developed mainly at relatively high wind velocities on wet to moist substrata, but were less pronounced under water. The structure of these deposits is, however, different from those produced by running water. Thin section analysis of eolian accumulations on a dry substratum showed no lamination, with mineral- or size-sorting phenomena." @default.
- W70950068 created "2016-06-24" @default.
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- W70950068 date "1990-01-01" @default.
- W70950068 modified "2023-09-26" @default.
- W70950068 title "Sedimentary Structures Formed in Eolian-Deposited Silt Loams Under Simulated Conditions on Dry, Moist and Wet Surfaces" @default.
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- W70950068 doi "https://doi.org/10.1016/s0166-2481(08)70325-8" @default.
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